From the Late Triassic Riograndia Assemblage Zone (Santa Maria Supersequence) of Southern Brazil

Total Page:16

File Type:pdf, Size:1020Kb

From the Late Triassic Riograndia Assemblage Zone (Santa Maria Supersequence) of Southern Brazil Anais da Academia Brasileira de Ciências (2014) 86(4): 1673-1691 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201420140455 www.scielo.br/aabc A new prozostrodontian cynodont (Therapsida) from the Late Triassic Riograndia Assemblage Zone (Santa Maria Supersequence) of Southern Brazil MARINA B. SOARES1, AGUSTÍN G. MARTINELLI1 and TÉO V. DE OLIVEIRA2 1Laboratório do Setor de Paleovertebrados, Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, Universidade Federal do Rio Grande do Sul/UFRGS, Av. Bento Gonçalves, 9500, 90540-000 Porto Alegre, RS, Brasil 2Museu de Zoologia, Departamento de Ciências Biológicas, Universidade Estadual de Feira de Santana/UEFS, Av. Transnordestina, s/n, Novo Horizonte, 44036-900 Feira de Santana, BA, Brasil Manuscript received on September 8, 2014; accepted for publication on October 14, 2014 ABSTRACT We report here on a new prozostrodontian cynodont, Botucaraitherium belarminoi gen. et sp. nov., from the Late Triassic Riograndia Assemblage Zone (AZ) of the Candelária Sequence (Santa Maria Supersequence), collected in the Botucaraí Hill Site, Candelária Municipality, state of Rio Grande do Sul, Brazil. The new taxon is based on a single specimen (holotype MMACR-PV-003-T) which includes the left lower jaw, without postdentary bones, bearing the root of the last incisor, canine and four postcanines plus one partial crown inside the dentary, not erupted, and two maxillary fragments, one with a broken canine and another with one postcanine. The features of the lower jaw and lower/upper postcanines resemble those of the prozostrodontians Prozostrodon brasiliensis from the older Hyperodapedon AZ and Brasilodon quadrangularis and Brasilitherium riograndensis from the same Riograndia AZ. The inclusion of Botucaraitherium within a broad phylogenetic analysis, positioned it as a more derived taxon than tritylodontids, being the sister-taxon of Brasilodon, Brasilitherium plus Mammaliaformes. Although the new taxon is based on few cranial elements, it represents a additional faunal component of the Triassic Riograndia AZ of southern Brazil, in which small-sized derived non-mammaliaform cynodonts, closely related to the origin of mammaliaforms, were ecologically well succeed and taxonomically diverse. Key words: Cynodontia, Prozostrodontia, Santa Maria Supersequence, Triassic. INTRODUCTION based on correlations with Argentinean and The rich fossil tetrapod content from the Middle- Malagasy faunas (Abdala and Ribeiro 2010), Upper Triassic of southern Brazil is recorded in the non-mammaliaform cynodonts (Therapsida, beds related to the Santa Maria Supersequence, in Eucynodontia) account for a significant percentage which four recognized faunal tetrapod associations of the recorded taxa, taxonomically comprising succeed in time: Dinodontosaurus, Santacruzodon, the most diverse group. In fact, the diversity of the Hyperodapedon and Riograndia Assemblage Zones derived non-mammaliaform probainognathian (AZ) (Soares et al. 2011) (Fig. 1). In all of these cynodonts, grouped into the Clade Prozostrodontia bio stratigraphic unities, whose proposed ages are (sensu Liu and Olsen 2010), from the Upper Triassic Candelária Sequence (Santa Maria Supersequence) Correspondence to: Marina Bento Soares E-mail: [email protected] of southern Brazil is remarkable when compared to An Acad Bras Cienc (2014) 86 (4) 1674 MARINA B. SOARES, AGUSTÍN G. MARTINELLI and TÉO V. DE OLIVEIRA its global fossil record, based upon poorly preserved Bonaparte et al. (2003), and Minicynodon specimens. At least two prozostrodontians are Bonaparte et al. (2010). Riograndia is the most known from the Hyperodapedon AZ (Bonaparte and common cynodont of this AZ, represented Barberena 2001) and at least five from the younger by several exquisitely preserved specimens. Riograndia AZ (Bonaparte et al. 2001, 2003, 2005, Riograndia is considered as a basal member of 2010, 2012, Martinelli et al. 2005, Soares et al. 2011). the Tritheledontidae Clade (Bonaparte et al. 2001, Recent studies on these taxa have highlighted their Soares et al. 2011) or a basal Ictidosauria, sister- essential contribution to the understanding of the taxon of Tritheledontidae (sensu Martinelli et al. mammaliaforms origin (Bonaparte et al. 2005, Luo 2005, Martinelli and Rougier 2007). Irajatherium 2007, Abdala 2007, Liu and Olsen 2010, Bonaparte is still poorly represented in comparison to other 2012), illustrating the climbing mosaic of characters cynodonts from this AZ. However, its dentition developed during the Middle-Late Triassic transition resembles that of Chaliminia from the Late (Bonaparte et al. 2005, Martinelli and Rougier 2007, Triassic of Argentina and Pachygenelus from the Martinelli and Bonaparte 2011, Bonaparte 2012, Early Jurassic of Africa (Martinelli and Rougier Rodrigues et al. 2012, 2013). 2007). Hence, Irajatherium is positioned as a basal In the late Carnian Hyperodapedon AZ, Tritheledontidae (Martinelli et al. 2005, Martinelli the prozostrodontians Therioherpeton cargnini and Rougier 2007, Oliveira et al. 2011). Brasilodon, Bonaparte and Barberena (1975) and Prozostrodon Brasilitherium (Bonaparte et al. 2003, 2005, brasiliensis Bonaparte and Barberena (2001) are 2012), and Minicynodon (Bonaparte et al. 2010, recognized, both displaying several derived features 2012) are relatively well-documented and they are in the skull and dentition (e.g. lack of prefrontal crucial taxa in cynodont evolution because they and postorbital, constricted root in postcanines) constitute the sister-group of Mammaliaformes that positioned them as basal prozostrodontians (e.g., Bonaparte et al. 2003, 2005, 2012, Abdala (Liu and Olsen 2010). From this AZ, Charruodon 2007, Martinelli and Rougier 2007, Luo 2007, Liu tetracuspidatus Abdala and Ribeiro (2000) and and Olsen 2010, Rodrigues et al. 2012, 2013, Ruff Trucidocynodon riograndensis Oliveira et al. et al. 2014). Bonaparte et al. (2005) created the (2010) are also known. Charruodon was originally Family Brasilodontidae to include Brasilodon and related to Therioherpeton due to the morphology Brasilitherium, and, subsequently, other taxa were of the lower postcanines; nonetheless, based on included in it such as Protheriodon estudianti the deep and robust lower jaw (unexpected for (Bonaparte et al. 2006, Bonaparte 2012). Some Therioherpeton based on its skull), we consider that authors (e.g., Liu and Olsen 2010) pointed out the phylogenetic position of Charruodon cannot be that Brasilodon and Brasilitherium are synonym elucidated until new specimens come to light. On the and also that a monophyletic Brasilodontidae other hand, Trucidocynodon represents a member of has not been recovered (e.g., Abdala 2007). the Ecteniniidae (Oliveira et al. 2010, Martinez et al. Notwithstanding these issues that are currently 2013), which is positioned outside, as sister-group of under revision, the impact that the discovery of Prozostrodontia (Martinez et al. 2013). the brasilodontids from the Riograndia AZ of With regard to the prozostrodontian content, the southern Brazil has caused is unprecedented early Norian Riograndia AZ includes Riograndia (Bonaparte et al. 2003, 2005, 2012, Rodrigues et guaibensis Bonaparte et al. (2001) Irajatherium al. 2012, 2013). hernandezi Martinelli et al. (2005), Brasilodon In this contribution, we present a new pro- quadrangularis, Brasili therium riograndensis zostrodontian cynodont from the Riograndia AZ of An Acad Bras Cienc (2014) 86 (4) A NEW CYNODONT FROM THE LATE TRIASSIC OF BRAZIL 1675 the Candelária Municipality, state of Rio Grande with several features shared with Prozostrodon do Sul, Brazil. The new taxon is described, from the Hyperodapedon AZ and especially compared and included in a broad phylogenetic with Brasilodon and Brasilitherium from the analysis of cynodonts. Although based on a partial Riograndia AZ. The new specimen contributes lower jaw and maxillary fragments, the specimen to the understanding of the non-mammaliaform represents a new taxon of prozostrodontian prozostrodontian diversity. Fig. 1 - A: Geographical location of the Santa Maria Supersequence (Paraná Basin) in the state of Rio Grande do Sul, Brazil. B: Chronostratigraphy of the southern Brazilian Triassic, showing the four Assemblage Zones (AZ) based on tetrapods context. From Horn et al. 2004. Biostratigraphy after Soares et al. 2011. Abbreviations: Any, Anisian; Car, Carnian; Ind, Induan; Lad, Ladinian; Nor, Norian; Ole, Olenekian; Rha, Rhaetian. GEOLOGICAL SETTING AND BIOSTRATIGRAPHY and Scherer 2000, Zerfass et al. 2003). The Candelária Sequence encompasses the Hyperodapedon AZ The Upper Triassic Candelária Sequence corresponds (sensu Abdala et al. 2001), in which the most abundant to a third-order sequence placed in the Santa Maria components are the rhynchosaur Hyperodapedon Supersequence (sensu Zerfass et al. 2003, Horn et sp. and the traversodontid cynodont Exaeretodon al. 2014) (Fig. 1). The basal portion of the Sequence riograndensis Abdala et al. (2002). Besides the consists of a coarsening-upward succession that begins aforementioned cynodonts (e.g., Trucidocynodon, with red mudstones interbedded with small-scale Therioherpeton, Charruodon and Prozostrodon), its trough cross-bedded sandstone lenses. Rhytmites dinosaur content also deserves mention (Bittencourt and sigmoidal massive to climbing cross-laminated and Kellner 2009, Langer et al. 1999, Cabreira et al. sandstone bodies are also present
Recommended publications
  • Ischigualasto Formation. the Second Is a Sile- Diversity Or Abundance, but This Result Was Based on Only 19 of Saurid, Ignotosaurus Fragilis (Fig
    This article was downloaded by: [University of Chicago Library] On: 10 October 2013, At: 10:52 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 Vertebrate succession in the Ischigualasto Formation Ricardo N. Martínez a , Cecilia Apaldetti a b , Oscar A. Alcober a , Carina E. Colombi a b , Paul C. Sereno c , Eliana Fernandez a b , Paula Santi Malnis a b , Gustavo A. Correa a b & Diego Abelin a a Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan , España 400 (norte), San Juan , Argentina , CP5400 b Consejo Nacional de Investigaciones Científicas y Técnicas , Buenos Aires , Argentina c Department of Organismal Biology and Anatomy, and Committee on Evolutionary Biology , University of Chicago , 1027 East 57th Street, Chicago , Illinois , 60637 , U.S.A. Published online: 08 Oct 2013. To cite this article: Ricardo N. Martínez , Cecilia Apaldetti , Oscar A. Alcober , Carina E. Colombi , Paul C. Sereno , Eliana Fernandez , Paula Santi Malnis , Gustavo A. Correa & Diego Abelin (2012) Vertebrate succession in the Ischigualasto Formation, Journal of Vertebrate Paleontology, 32:sup1, 10-30, DOI: 10.1080/02724634.2013.818546 To link to this article: http://dx.doi.org/10.1080/02724634.2013.818546 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content.
    [Show full text]
  • O Esqueleto Pós-Craniano De Exaeretodon Riograndensis Abdala Et Al
    Rev. bras. paleontol. 10(2):79-94, Maio/Agosto 2007 © 2007 by the Sociedade Brasileira de Paleontologia O ESQUELETO PÓS-CRANIANO DE EXAERETODON RIOGRANDENSIS ABDALA ET AL. (CYNODONTIA, TRAVERSODONTIDAE), TRIÁSSICO DO BRASIL TÉO VEIGA DE OLIVEIRA, CESAR LEANDRO SCHULTZ & MARINA BENTO SOARES Instituto de Geociências, UFRGS, Avenida Bento Gonçalves, 9500, 91501-970, Porto Alegre, RS, Brasil. [email protected], [email protected], [email protected] RESUMO – Pela primeira vez, elementos pós-cranianos de Exaeretodon riograndensis, um cinodonte traversodontídeo da Cenozona de Rhynchosauria da Formação Santa Maria, Neotriássico do sul do Brasil, são descritos e comparados com E. frenguellii e outros cinodontes não-mamalianos. O material inclui parte da coluna vertebral, radio, ulna e elementos da cintura pélvica. As diferenças mais significativas em relação a E. frenguellii estão na morfologia e nas dimensões do arco neural do atlas, na presença de intercentros em vértebras cervicais posteriores ao áxis e na ausência da dilatação do ápice do espinho neural das vértebras truncais. A morfologia da região sacral da coluna, do rádio, da ulna e da cintura pélvica são concordantes com o observado em E. frenguellii. A comparação com outros táxons de cinodontes não-mamalianos permite a observação da nítida evolução em mosaico do esqueleto pós-craniano destes animais: E. riograndensis mostra alguns caracteres similares a outros Cynognathia (grupo ao qual pertence), enquanto outros são mais próximos aos observados em alguns Probainognathia (incluindo mamíferos), como a natureza mais avançada do complexo atlas-áxis. Palavras-chave: Triássico, Brasil, Formação Santa Maria, Traversodontidae, Exaeretodon riograndensis, pós-crânio. ABSTRACT – THE POSTCRANIAL SKELETON OF EXAERETODON RIOGRANDENSIS ABDALA ET AL.
    [Show full text]
  • Micheli Stefanello
    UNIVERSIDADE FEDERAL DE SANTA MARIA CENTRO DE CIÊNCIAS NATURAIS E EXATAS PROGRAMA DE PÓS-GRADUAÇÃO EM BIODIVERSIDADE ANIMAL Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Santa Maria, RS 2018 Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Dissertação apresentada ao Curso de Mestrado do Programa de Pós-Graduação em Biodiversidade Animal, Área de Concentração em Sistemática e Biologia Evolutiva, da Universidade Federal de Santa Maria (UFSM, RS), como requisito parcial para obtenção do grau de Mestre em Ciências Biológicas – Área Biodiversidade Animal. Orientador: Prof. Dr. Sérgio Dias da Silva Santa Maria, RS 2018 Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Dissertação apresentada ao Curso de Mestrado do Programa de Pós-Graduação em Biodiversidade Animal, Área de Concentração em Sistemática e Biologia Evolutiva, da Universidade Federal de Santa Maria (UFSM, RS), como requisito parcial para obtenção do grau de Mestre em Ciências Biológicas – Área Biodiversidade Animal. Aprovada em 28 de fevereiro de 2018: Santa Maria, RS 2018 AGRADECIMENTOS Ao meu orientador, Dr. Sérgio Dias da Silva, pela orientação, por todo o tempo despendido ao longo desse mestrado e por possibilitar meu aprimoramento na área a qual tenho apreço. Aos colegas do Centro de Apoio à Pesquisa Paleontológica da Quarta Colônia da Universidade Federal de Santa Maria (CAPPA/UFSM) e do Laboratório de Paleobiodiversidade Triássica, dessa mesma instituição, pela convivência e por terem ajudado-me de diferentes formas ao longo do mestrado. Em especial, ao colega Rodrigo Temp Müller, pela coleta do espécime (objeto de estudo dessa dissertação), por toda a ajuda com o TNT e com as figuras, e por auxiliar-me de inúmeras formas.
    [Show full text]
  • Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
    Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages.
    [Show full text]
  • Um Novo E Peculiar Cinodonte Traversodontídeo Para O Triássico Médio Do Rio Grande Do Sul E Suas Implicações Para a Paleoecologia De
    UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS Um Novo e Peculiar Cinodonte Traversodontídeo para o Triássico Médio do Rio Grande do Sul e suas Implicações para a Paleoecologia de Cynodontia Míriam Reichel Orientador: Prof. Dr. Cesar Leandro Schultz Co-Orientadora: Profª. Drª. Marina Bento Soares Comissão Examinadora: Prof. Dr. José Fernando Bonaparte Prof. Dr. Mario Cozzuol Profª. Drª. Cristina Vega Dias Dissertação de Mestrado apresentada como requisito para obtenção do título de Mestre em Ciências Livros Grátis http://www.livrosgratis.com.br Milhares de livros grátis para download. Reichel, Miriam Um novo e peculiar Cinodonte Traversodontídeo para triássico médio do Rio Grande do Sul e suas implicações para a Paleoecologia de Cynodontia. / Miriam Reichel. - Porto Alegre : UFRGS, 2006. [145 f.] il. Dissertação (Mestrado). - Universidade Federal do Rio Grande do Sul. Instituto de Geociências. Programa de Pós-Graduação em Geociências. Porto Alegre, RS - BR, 2006. 1. Paleoecologia. 2. Cynodontia. 3. Traversodontidae. 4. Triássico Médio. 5. Formação Santa Maria. 6. Rio Grande do Sul. I. Título. _____________________________ Catalogação na Publicação Biblioteca Geociências - UFRGS Renata Cristina Grun CRB 10/1113 AGRADECIMENTOS • Ao professor Dr. José Fernando Bonaparte, pelos ensinamentos a respeito dos cinodontes, por estimular este trabalho, contribuindo com importantes comentários, e pela grande dedicação à paleontologia e àqueles que por ela se interessam. • Ao professor Dr. Cesar Leandro Schultz, por orientar este trabalho, por sempre tornar o ambiente de trabalho agradável, pelos conselhos e pela amizade. • À professora Dra. Marina Bento Soares, por me trazer para o mundo dos cinodontes, pela paciência e didática de fundamental importância para este trabalho, pelo carinho e pela amizade.
    [Show full text]
  • Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
    438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna.
    [Show full text]
  • Um Novo E Peculiar Cinodonte Traversodontídeo Para O Triássico Médio Do Rio Grande Do Sul E Suas Implicações Para a Paleoecologia De
    UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS Um Novo e Peculiar Cinodonte Traversodontídeo para o Triássico Médio do Rio Grande do Sul e suas Implicações para a Paleoecologia de Cynodontia Míriam Reichel Orientador: Prof. Dr. Cesar Leandro Schultz Co-Orientadora: Profª. Drª. Marina Bento Soares Comissão Examinadora: Prof. Dr. José Fernando Bonaparte Prof. Dr. Mario Cozzuol Profª. Drª. Cristina Vega Dias Dissertação de Mestrado apresentada como requisito para obtenção do título de Mestre em Ciências Reichel, Miriam Um novo e peculiar Cinodonte Traversodontídeo para triássico médio do Rio Grande do Sul e suas implicações para a Paleoecologia de Cynodontia. / Miriam Reichel. - Porto Alegre : UFRGS, 2006. [145 f.] il. Dissertação (Mestrado). - Universidade Federal do Rio Grande do Sul. Instituto de Geociências. Programa de Pós-Graduação em Geociências. Porto Alegre, RS - BR, 2006. 1. Paleoecologia. 2. Cynodontia. 3. Traversodontidae. 4. Triássico Médio. 5. Formação Santa Maria. 6. Rio Grande do Sul. I. Título. _____________________________ Catalogação na Publicação Biblioteca Geociências - UFRGS Renata Cristina Grun CRB 10/1113 AGRADECIMENTOS • Ao professor Dr. José Fernando Bonaparte, pelos ensinamentos a respeito dos cinodontes, por estimular este trabalho, contribuindo com importantes comentários, e pela grande dedicação à paleontologia e àqueles que por ela se interessam. • Ao professor Dr. Cesar Leandro Schultz, por orientar este trabalho, por sempre tornar o ambiente de trabalho agradável, pelos conselhos e pela amizade. • À professora Dra. Marina Bento Soares, por me trazer para o mundo dos cinodontes, pela paciência e didática de fundamental importância para este trabalho, pelo carinho e pela amizade. • Às colegas Paula C.
    [Show full text]
  • Paleontologia Em Destaque
    Paleontologia em Destaque Boletim Informativo da SBP Ano 34, n° 72, 2019 · ISSN 1807-2550 PALEO, SBPV e SBPI 2018 RELATOS E RESUMOS SOCIEDADE BRASILEIRA DE PALEONTOLOGIA Presidente: Dr. Renato Pirani Ghilardi (UNESP/Bauru) Vice-Presidente: Dr. Annie Schmaltz Hsiou (USP/Ribeirão Preto) 1ª Secretária: Dra. Taissa Rodrigues Marques da Silva (UFES) 2º Secretário: Dr. Rodrigo Miloni Santucci (UnB) 1º Tesoureiro: Me. Marcos César Bissaro Júnior (USP/Ribeirão Preto) 2º Tesoureiro: Dr. Átila Augusto Stock da Rosa (UFSM) Diretor de Publicações: Dr. Sandro Marcelo Scheffler (UFRJ) P a l e o n t o l o g i a e m D e s t a q u e Boletim Informativo da Sociedade Brasileira de Paleontologia Ano 34, n° 72, setembro/2019 · ISSN 1807-2550 Web: http://www.sbpbrasil.org/, Editores: Sandro Marcelo Scheffler, Maria Izabel Lima de Manes Agradecimentos: Aos organizadores dos eventos científicos Capa: Palácio do Museu Nacional após a instalação do telhado provisório. Foto: Sandro Scheffler. 1. Paleontologia 2. Paleobiologia 3. Geociências Distribuído sob a Licença de Atribuição Creative Commons. EDITORIAL As reuniões PALEO são encontros regionais chancelados pela Sociedade Brasileira de Paleontologia (SBP) que têm por objetivo a comunhão entre estudantes de graduação e pós- graduação, pesquisadores e interessados na área de Paleontologia. Estes eventos possuem periodicidade anual e ocorrem em várias regiões do Brasil. Iniciadas em 1999, como uma reunião informal da comunidade de paleontólogos, possuem desde então as seguintes distribuições, de acordo com a região de abrangência: Paleo RJ/ES, Paleo MG, Paleo SP, Paleo RS, Paleo PR/SC, Paleo Nordeste e Paleo Norte.
    [Show full text]
  • Evolution of the Mammalian Fauces Region and the Origin of Suckling
    Evolution of the mammalian fauces region and the origin of suckling The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Crompton, Alfred, Catherine Musinsky, Jose Bonaparte, Bhart- Anjan Bhullar, and Tomasz Owerkowicz. Evolution of the mammalian fauces region and the origin of suckling (2018). Citable link https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37364482 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA 1 Evolution of the mammalian fauces region and the origin of suckling Alfred Crompton1†, Catherine Musinsky1, Jose Bonaparte2, Bhart-Anjan Bhullar3, Tomasz Owerkowicz4 1: Harvard University, Organismic and Evolutionary Biology Department, Museum of Comparative Zoology, 26 Oxford St, Cambridge, MA 02138 USA 2: Museo Municipal de C. Naturales "C. Ameghino", 6600 MERCEDES – BS. AS. Argentina 3: Department of Geology & Geophysics, Yale University, PO Box 208109, New Haven, CT 06520- 8109 USA 4: Department of Biology, California State University in San Bernadino, 5500 University Pkwy, San Bernardino, CA 92407 USA †corresponding author: ORCID 0000-0001-6008-2587, [email protected], 617-495-3202 Acknowledgments Thanks to Dr. Edgar Allin for his comments on an early draft of this paper. Thanks to the Museum of Comparative Zoology, its Director, Professor James Hanken, and to the Center for Nanoscale Systems at Harvard University for providing the facilities and finances for this research.
    [Show full text]
  • Osteohistology of Late Triassic Prozostrodontian Cynodonts from Brazil
    Osteohistology of Late Triassic prozostrodontian cynodonts from Brazil Jennifer Botha-Brink1,2, Marina Bento Soares3 and Agustín G. Martinelli3 1 Department of Karoo Palaeontology, National Museum, Bloemfontein, South Africa 2 Department of Zoology and Entomology, University of the Free State, Bloemfontein, South Africa 3 Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil ABSTRACT The Prozostrodontia includes a group of Late Triassic-Early Cretaceous eucynodonts plus the clade Mammaliaformes, in which Mammalia is nested. Analysing their growth patterns is thus important for understanding the evolution of mammalian life histories. Obtaining material for osteohistological analysis is difficult due to the rare and delicate nature of most of the prozostrodontian taxa, much of which comprises mostly of crania or sometimes even only teeth. Here we present a rare opportunity to observe the osteohistology of several postcranial elements of the basal prozostrodontid Prozostrodon brasiliensis, the tritheledontid Irajatherium hernandezi, and the brasilodontids Brasilodon quadrangularis and Brasilitherium riograndensis from the Late Triassic of Brazil (Santa Maria Supersequence). Prozostrodon and Irajatherium reveal similar growth patterns of rapid early growth with annual interruptions later in ontogeny. These interruptions are associated with wide zones of slow growing bone tissue. Brasilodon and Brasilitherium exhibit a mixture of woven-fibered bone tissue and slower growing parallel-fibered and lamellar bone. The slower growing bone tissues are present even during early ontogeny. The relatively slower growth in Brasilodon and Brasilitherium may be related to their small body size compared to Prozostrodon and Irajatherium. These brasilodontids also exhibit osteohistological similarities with the Late Triassic/Early Jurassic mammaliaform Morganucodon and the Late Cretaceous multituberculate mammals Kryptobaatar and Nemegtbaatar.
    [Show full text]
  • A New Mammaliaform from the Early Jurassic and Evolution Of
    R EPORTS tary trough with a shelflike dorsal medial ridge, and all other nonmammalian mamma- A New Mammaliaform from the liaforms have a medial concavity on the man- dibular angle (8–14, 23), as in nonmamma- Early Jurassic and Evolution of liaform cynodonts (9, 14, 24–27). The post- dentary trough and the medial concavity on Mammalian Characteristics the mandibular angle respectively accommo- dated the prearticular/surangular and the re- Zhe-Xi Luo,1* Alfred W. Crompton,2 Ai-Lin Sun3 flected lamina of the angular (9, 25–27) that are the homologs to the mammalian middle A fossil from the Early Jurassic (Sinemurian, ϳ195 million years ago) represents ear bones (9, 14, 16–21, 23, 26). The absence a new lineage of mammaliaforms, the extinct groups more closely related to of these structures indicates that the postden- the living mammals than to nonmammaliaform cynodonts. It has an enlarged tary bones (“middle ear ossicles”) must have cranial cavity, but no postdentary trough on the mandible, indicating separation been separated from the mandible (Fig. 3). of the middle ear bones from the mandible. This extends the earliest record of Hadrocodium lacks the primitive meckelian these crucial mammalian features by some 45 million years and suggests that sulcus of the mandible typical of all nonmam- separation of the middle ear bones from the mandible and the expanded brain maliaform cynodonts (24–27), stem groups vault could be correlated. It shows that several key mammalian evolutionary of mammaliaforms (8, 9, 14, 23, 26, 27), innovations in the ear region, the temporomandibular joint, and the brain vault triconodontids (28, 29), and nontribosphenic evolved incrementally through mammaliaform evolution and long before the therian mammals (30).
    [Show full text]
  • Mesozoic: the Dark Age for Mammals!
    Ed’s Simplified History of the Mammals Note progression from Pelycosaurs (1) to Therapsids and Cynodonts (2) in Triassic. Stem mammals appeared in Late Triassic and Early Jurassic (3). Relationships among the Middle Jurassic forms (4) are controversial (see handout). Therian clade, identified by the tribosphenic molar (5), emerged at the end of the Jurassic, Early Cretaceous. A slightly more detailed version… in case you like something that looks more slick From Pough et al. 2009. Vertebrate Life, 8th ed. Pelycosaurs Dominated the late Permian, gave rise to therapsids Therapsids Rapid radiation in late Permian, around 270 MYA Still “mammal-like reptiles” The mass extinction at the end of the Permian was the greatest loss of diversity ever with >80% of all known genera and about 90% of all species going extinct, both terrestrial and marine. Cynodonts Late Permian to mid Triassic Last remaining group of therapsids, survived mass extinction at the end of the Permian. Persisted well Only 1 lineage of into Triassic and developed cynodonts survived many features associated through the late Triassic, with mammals. and this group became ancestors of mammals. Mesozoic: the Dark Age for Mammals! multituberculate Morganucodon, one of the earliest mammals (What else was happening in the Late Triassic and Jurassic Hadrocodium that may have contributed to mammals becoming small and Most were very small with nocturnal?) conservative morphology ...but new fossil finds indicate more diversity than we thought Repenomanus Still, largest known mammal during Mesozic Most were shrew to is no larger than a mouse sized, for 125 woodchuck million years! Some Mesozoic events and mammals you should know 1.
    [Show full text]